Crop coefficient and ratio of transpiration to evapotranspiration of winter wheat and maize in a semi-humid region

被引:314
作者
Kang, SZ
Gu, BJ
Du, TS
Zhang, JH
机构
[1] NW A&F Univ, Key Lab Agr Soil & Water Engn Arid & Semi Arid Ar, Minist Educ, Yangling 712100, Shaanxi, Peoples R China
[2] China Agr Univ, Coll Water Resources & Civil Engn, Beijing 100084, Peoples R China
[3] Minist Water Resources, Dept Rural Water Conservancy, Beijing 100053, Peoples R China
[4] Hong Kong Baptist Univ, Dept Biol, Hong Kong, Hong Kong, Peoples R China
关键词
crop coefficient; evapotranspiration; transpiration; leaf area index; wheat (Triticum aestivum); maize (Zea mays);
D O I
10.1016/S0378-3774(02)00150-6
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Crop coefficient (K-c) is an important parameter for irrigation scheduling and water allocation. This study investigated and determined the crop coefficients and the ratio of transpiration to evapotranspiration (T-p/ETc) of winter wheat (Triticum aestivum L.) and maize (Zea Mays) based on lysimeter data for 10 years in a semi-arid region of northwest China (34degrees20'N, 108degrees24'E). Several relationships, K-c and days after sowing (DAS), K-c and leaf area index (LAI), and T-p/ETc and LAI, were also analyzed. The average seasonal ETc for winter wheat and maize were 443.6 and 424.0 mm, respectively, compared to their reference crop evapotranspiration (ET0), 483.9 and 407.7 mm, respectively, for their seasons. The seasonal transpiration accounted for 67.0 and 74.0% of their evapotranspiration for winter wheat and maize, respectively. The average, maximum and minimum seasonal K-c were 0.92, 1.33 and 0.42, respectively, for winter wheat, and 1.04, 1.43 and 0.45, respectively, for the maize. The relationship between K-c and DAS was fitted to a fifth-order polynomial equation with significant correlation coefficients, R-2 = 0.960 and 0.980, respectively, for wheat and maize. The maximum K-c occurred at about 200 and 80 DAS for winter wheat and maize, respectively. K-c and LAI showed a saturation relationship, R-2 = 0.861 and 0.952, respectively, for wheat and maize, and K-c exceeded 1.0 when LAI was larger than 2.5 for both crops. The T-p/ETc and LAI also showed saturation relationship, R-2 = 0.968 and 0.981, respectively, for wheat and maize. T-p/ETc started from 0 at sowing, and reached to its maximum, near 0.9, at the middle growth stage or when LAI reached to about 3.0 for both crops. T-p/ETc maintained at its maximum when LAI was larger than 3.0. These results should help the precise planning and efficient management of irrigation for these crops in this region. (C) 2002 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:239 / 254
页数:16
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